Steen's theory on uranium deposits was that they would collect in anticlinal structures in the same manner as oil, which others on the Plateau dismissed as " Steen's Folly ."
42.
They are the surface expression of an anticlinal structure which continues to the south as the Kettleman Hills, and to the north as Anticline Ridge, a portion of the huge Coalinga Oil Field.
43.
Continued shortening and excess material within the anticlinal core not only results in increased amplitude and disharmonic folds, but may lead to the onset of thrusts out of the folded synclinal or anticlinal regions.
44.
Continued shortening and excess material within the anticlinal core not only results in increased amplitude and disharmonic folds, but may lead to the onset of thrusts out of the folded synclinal or anticlinal regions.
45.
"' Nittany Mountain "'is part of a synclinal depression of the anticlinal Nittany Arch, which originally formed a huge mountain, that has since eroded, during the Appalachian orogeny.
46.
The Baldwin Hills area had tempted drillers for years, but all early attempts to find oil were unsuccessful, probably because erosion and faulting made the anticlinal structure appear farther east than it really was.
47.
Anticline Ridge is the surface expression of an anticlinal structure which continues to the south as the Guijarral Hills and Kettleman Hills, and is the location of a major part of the huge Coalinga Oil Field.
48.
In 1983, Unocal discovered the Northwest Area, a small but productive region about a mile and a half northwest of the main part of the field, following the anticlinal trend of the hills, on the Jesus Maria lease.
49.
Folding also can provide tension, such as along the top of an anticlinal fold axis, where the tensile forces associated with the stretching of the upper half of the layers during folding can induce tensile fractures parallel to the fold axis.
50.
Folding initiates by shortening; limb lengthening and rotation and hinge migration, cause synclinal deflection below its original position accompanied by the flow of ductile material beneath the synclinal trough to the anticlinal core; resulting in increased amplitude of the anticlinal fold.
